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Monitoring Mount Sinabung in Indonesia Using Multi- Temporal Insar

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Monitoring Mount Sinabung in Indonesia Using Multi- Temporal Insar Korean Journal of Remote Sensing, Vol.33, No.1, 2017, pp.37~46 ISSN 1225-6161 ( Print ) http://dx.doi.org/10.7780/kjrs.2017.33.1.4 ISSN 2287-9307 (Online) Article Monitoring Mount Sinabung in Indonesia Using Multi- Temporal InSAR Chang-Wook Lee*, Zhong Lu** and Jin Woo Kim** † * Division of Science Education, College of Education, Kangwon National University ** Roy M Huffington Department of Earth Sciences, Southern Methodist University Sinabung volcano in Indonesia was formed due to the subduction between the Eurasian and Abstract : Indo-Australian plates along the Pacific Ring of Fire. After being dormant for about 400 years, Sinabung volcano erupted on the 29th of August, 2010 and most recently on the 1st of November, 2016. We measured the deformation of Sinabung volcano using Advanced Land Observing Satellite/Phased Array type L-band Synthetic Aperture Radar (ALOS/PALSAR) interferometric synthetic aperture radar (InSAR) images acquired from February 2007 to January 2011. Based on multi-temporal InSAR processing, we mapped the ground surface deformation before, during, and after the 2010 eruption with time-series InSAR technique. During the 3 years before the 2010 eruption, the volcano inflated at an average rate of ~1.7 cm/yr with a markedly higher rate of 6.6 cm/yr during the 6 months prior to the 2010 eruption. The inflation was constrained to the top of the volcano. From the 2010 eruption to January 2011, the volcano subsided by approximately 3 cm (~6 cm/yr). We interpreted that the inflation was due to magma accumulation in a shallow reservoir beneath Sinabung. The deflation was attributed to magma withdrawal from the shallow reservoir during the eruption as well as thermo-elastic compaction of erupted material. This result demonstrates once again the utility of InSAR for volcano monitoring. Sinabung volcano, surface deformation, InSAR, time-series Key Words : 1. Introduction significant seismic and volcanic activity. The Island of Sumatra has been the location for three of the world’s The Island of Sumatra is located along a segment of twelve largest earthquakes all with magnitudes higher the “Ring of Fire”, on the northern boundary of the than Mw 8.5. The 2004 Sumatra earthquake, which is Australian plate and the southern boundary of the the third largest earthquake (Mw 9.1), was particularly Eurasian plate (Global Volcanism Program). From the devastating because it was accompanied by a tsunami geologic record it is apparent that during the past 2.5 that killed more than 227,000 people from 14 countries million years, this region has been experiencing in South Asia and East Africa. The largest eruption Received February 9, 2017; Revised February 10, 2017; Accepted February 11, 2017. † Corresponding Author: Jin Woo Kim ([email protected]) This is an Open-Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons. org/licenses/by-nc/3.0) which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited –37 – Korean Journal of Remote Sensing , Vol .33, No .1, 2017 event in this region, with a volcanic explosivity index volcano has been poorly monitored. The latest eruption (VEI) of 8, occurred between 69,000 and 77,000 years at Sinabung began on the 29th of August, 2010. This ago at Toba volcano on the Island of Sumatra, less than explosive eruption produced ash plumes rising several 50 km southeast of Sinabung. kilometers above the crater and forced the evacuation Mount Sinabung is a stratovolcano in the of 20,000 to 30,000 people within a 6 km radius of the northwestern part of the Island of Sumatra in Indonesia volcano. Two individual ash plumes from separate vents (Fig. 1a). The volcano was formed during the near the summit were produced during this eruption, one Pleistocene to Holocene and consists of andesitic and vertical and one horizontal (Figs. 2a and b). Explosions dacitic lavas. Sinabung’s 2,460-m-high conical structure and ash plumes accompanied by strong volcanic has four overlapping craters (Global Volcanism tremors, which were felt by residents as far as 8 km Program). It is mostly covered with dense vegetation away, continued until the 22nd of September. and only the top of the volcano is free of vegetation (Fig. According to the Center of Volcanology and Geological 1b). The four summit vents are elongated from north- Hazard Mitigation (CVGHM), the ash plume, over the south and range from 60 m to 300 m in diameter (Figs. duration of this eruptio n, reached a maximum height of 1c and d). Little is known about the volcano’s eruption 5 km above the crater floor on the 7th of September. history, but the last historical eruption occurred around The volcano remained dormant for another three 400 years ago. Because of this long dormancy, the years before erupting again on the 15th of September, Fig. 1. (a) Sinabung volcano, located in the northern region of the Island of Sumatra, Indonesia. (b) Landsat-7 image acquired on May 19, 2003 of the Mount Sinabung area. (c) Averaged SAR amplitude image between January 1, 2007 and January 16, 2011. (d) Combined Landsat-7 and averaged SAR images. Red arrows indicate the location of multi-craters and the yellow dotted lines delineate the extent of the rocky area. –38 – Monitoring Mount Sinabung in Indonesia Using Multi-Temporal InSAR Fig. 2. Twin ash plumes from Sinabung volcano eruption of 29-30th of August, 2010. Picture by the Jakarta Post on the 29th of August (a) and the 30th of August (b). (c) Landsat 7 image (RGB = 3,2,1) acquired on September 11, 2013. 2013. During this eruption the ash plume rose to an Simons, 2004; Lu et al ., 2010; Lu and Dzurisin, 2014; altitude of 6.1 km, and 3,700 people within a 3-km Chaussard and Amelung, 2012; Ebmeier et al ., 2010; radius of the volcano were evacuated. Moreover, Philibosian and Simon, 2011; Furuta, 2009). Because volcanic ash fell as far away as 50 km from the volcano Sinabung is heavily vegetated, there is too much loss in the northeast direction. Landsat 7 satellite image of coherence in C-band InSAR imagery. However, (Fig. 2c) acquired 4 days before the eruption Chaussard and Amelung (2010, 2012) processed (September 11, 2013) shows a white ash cloud over the thirteen L-band ALOS/PALSAR images from summit of Sinabung and a grey volcanic ash plume on Sinabung, acquired before 2010 that show a the east side of the volcano. progressive rate of inflation of 2.2 cm/yr. In this study, The size of Sinabung volcano and the frequent and we used twenty ALOS/PALSAR data (Table 1) with complex nature of its eruptions make it difficult to study calibrated radar backscatter at HH polarization, the deformation that is occurring here using traditional including seven new images acquired in 2010 and methods that require surface based instruments. InSAR January 2011, to study deformation of the volcano. is an efficient method for measuring surface We applied a small baseline subset (SBAS) InSAR deformation over large areas (Massonnet and Feigl, technique (Berardino et al ., 2002; Lee et al ., 2011) to 1998; Rignot, 2008; Ng et al ., 2009; Lu et al ., 2009; estimate time-series surface deformation using a multi- Jung et al ., 2013a), and has been applied worldwide in interferogram processing approach (Rignot, 2008; Pan the study of volcanic deformation (Pritchard and and Tang, 2010). Atmospheric artifacts are reduced –39 – Korean Journal of Remote Sensing , Vol .33, No .1, 2017 Table 1. Characteristics of ALOS/PALSAR data used in this study Date Perpendicular Number Mission (Polarization) Orbit number (YYYYMMDD) baseline (m) 1 ALOS/PALSAR(HH) 00702 20070220 0 (M) 2 ALOS/PALSAR(HH) 00707 20070708 181(S) 3 ALOS/PALSAR(HH) 00708 20070823 205(S) 4 ALOS/PALSAR(HH) 00801 20080108 15(S) 5 ALOS/PALSAR(HH) 00802 20080223 194(S) 6 ALOS/PALSAR(HH) 00804 20080409 305(S) 7 ALOS/PALSAR(HH) 00805 20080525 -45(S) 8 ALOS/PALSAR(HH) 00810 20081010 -124(S) 9 ALOS/PALSAR(HH) 00901 20090110 101(S) 10 ALOS/PALSAR(HH) 00902 20090225 -227(S) 11 ALOS/PALSAR(HH) 00907 20090713 449(S) 12 ALOS/PALSAR(HH) 00908 20090828 546(S) 13 ALOS/PALSAR(HH) 00911 20091128 147(S) 14 ALOS/PALSAR(HH) 01001 20100113 -3(S) 15 ALOS/PALSAR(HH) 01002 20100228 189(S) 16 ALOS/PALSAR(HH) 01007 20100716 46(S) 17 ALOS/PALSAR(HH) 01008 20100831 202(S) 18 ALOS/PALSAR(HH) 01010 20101016 154(S) 19 ALOS/PALSAR(HH) 01012 20101201 -165(S) 20 ALOS/PALSAR(HH) 01101 20110116 31(S) •Perpendicular baseline (m): calculation perpendicular baseline information of Master (M) image corresponding to Slave (S) images respectively. through spatio-temporal filtering after the mean dataset, and then carried out the SBAS processing and deformation is obtained (Jung et al ., 2013b) and stacking to characterize the surface deformation of the iterative processing can further improve the time-series Sinabung volcano in spatio-temporal domain. Using deformation estimates (Lee et al ., 2011). When using twenty ALOS/PALSAR images from the 20th of this algorithm, the deformation for a specific time February, 2007 to the 16th of January, 2011 (Table 1), period can be calculated more precisely by minimizing we generated 39 interferograms (Fig. 3). all error components (Lee et al ., 2012). This technique Most of the interferograms had a perpendicular of a refined SBAS time-series analysis can successfully baseline of less than 400 m, but one interferogram had measure deformation with an error of 0.2 to 0.9 mm in a baseline of 550 m. The best coherence was the temporal domain and a root mean square error constrained on the volcano summit.
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